Permafrost and climatic change in China

• Published in: Global and planetary change Vol. 26; no. 4; pp. 387 - 404
• Main Authors: Jin, Huijun, Li, Shuxun, Cheng, Guodong, Shaoling, Wang, Li, Xin
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 15.12.2000
• Subjects: China; climatic change; degradation; environment; modeling; permafrost; China, People's Rep; climatic change; environment; degradation; modeling; permafrost; China
• ISSN: 0921-8181; 1872-6364
• DOI: 10.1016/S0921-8181(00)00051-5

The permafrost area in China is about 2.15×10 6 km 2, and is generally characterized by altitudinal permafrost. Permafrost in China can be divided into latitudinal and altitudinal types, the latter can be further divided into plateau and alpine permafrost. Altitudinal permafrost also can be divided into five thermal stability types. The permafrost environment has changed significantly since the Late Pleistocene. In northeastern China, the southern limit of permafrost extended to 41–42°N during the last glaciation maximum; in the Holocene megathermal, it retreated northward. The ice wedges and permafrost formed during the Late Pleistocene are still present in the northern part of the Da-Xing'anling Mountains. The inactive ice wedges at Yitulihe indicate a cooling and subsequent permafrost expansion during the Late Pleistocene. The lower limit of altitudinal permafrost in western China has elevated from 800 to 1500 m since the last glaciation maximum. Compared with that in northern Europe and North America, latitudinal permafrost in northeastern China is less sensitive to climatic warming, but altitudinal permafrost, especially permafrost on the Qinghai–Tibet Plateau (QTP), is sensitive to climatic warming. Since the early 20th century, significant permafrost degradation has occurred and is occurring in most permafrost regions in China. Due to the combined influence of climatic warming and increasing anthropogenic activities, substantial retreat of permafrost is expected on the QTP and in northeastern China during the 21st century. Permafrost degradation has and will cast great influence on engineering construction, water resources and environments in the cold regions of China. The wetlands in the cold regions of China emit significant amounts of CH 4 and N 2O to the atmosphere and uptake atmospheric CO 2 at a considerable rate, which might contribute to the global atmospheric carbon budget and feedback to climatic systems. However, uncertainties about permafrost changes, rates of changes and their environmental impacts are still large and call for intensive studying.